Movement is mostly in a vertical direction
tacitos
When movement occurs along a normal fault, the hanging wall moves down relative to the footwall. This type of faulting is caused by extensional stresses in the Earth's crust, where the crust is being pulled apart. Normal faults are common in areas of tectonic plate divergence or in regions experiencing crustal extension.
The sudden movement of the earth's crust is called and earthquake
The term that best describes the rocky outer layer of the Earth is the "crust." The Earth's crust is divided into two types: the oceanic crust, which is thinner and denser, and the continental crust, which is thicker and less dense.
Faults in earth science are fractures or discontinuities in the Earth's crust where there has been movement. This movement can be vertical, horizontal, or diagonal, and is caused by stress within the Earth's lithosphere. Faults are classified by the direction of movement as either normal (extensional), reverse (compressional), or strike-slip (lateral).
vertical direction
The movement of the crust along a thrust fault is usually a reverse movement unlike the movement along a normal fault.
The movement of the crust along a thrust fault is usually a reverse movement unlike the movement along a normal fault.
The movement of the Earth's crust along a slit or fracture is known as a "fault." Faults are caused by tectonic forces and can result in earthquakes. They are classified into different types, such as normal, reverse, and strike-slip faults, depending on the direction of movement.
These down-dropped blocks of crust are called grabens. Grabens are formed by the extensional forces that cause the crust to stretch and create space for the down-dropped blocks between the steeply dipping normal faults.
The term that describes down-dropped blocks of crust bounded by steeply dipping normal faults is "graben." Graben formations occur as a result of tectonic forces pulling the Earth's crust apart, leading to the subsidence of the block between the faults. This process is often associated with extensional tectonics and can create distinct geological features.
The term that describes down-dropped blocks of crust bounded by steeply dipping normal faults is "graben." Graben formations occur when tectonic forces cause the crust to extend and fracture, leading to the subsidence of these blocks. They are often found in rift valleys and are characterized by their steep sides and a lower elevation compared to the surrounding terrain.
Plate tectonic movement and subduction zones.
tacitos
When movement occurs along a normal fault, the hanging wall moves down relative to the footwall. This type of faulting is caused by extensional stresses in the Earth's crust, where the crust is being pulled apart. Normal faults are common in areas of tectonic plate divergence or in regions experiencing crustal extension.
the movement of earths plates or crust
The movement of magma through the Earth's crust is known as intrusion.